Document Details

Glaciers in California’s Sierra Nevada are likely disappearing for the first time in the Holocene

Andrew G. Jones, Shaun A. Marcott, Jeremy D. Shakun, Nathaniel A. Lifton, Andrew L. Gorin, Alan J. Hidy, Susan R. H. Zimmerman, Greg M. Stock, Tori M. Kennedy, Brent M. Goehring, Marc A. Caffee | October 1st, 2025


Mountain glaciers are sensitive climate indicators. Glaciers in the western United States are projected to disappear by 2100 CE, but whether they were previously absent in the current interglacial (past 11,700 years) remains debated. Here, we present evidence that two of the largest glaciers in California’s Sierra Nevada near Yosemite National Park persisted throughout the Holocene. Cosmogenic in situ carbon-14 and beryllium-10 exposure dating in newly exposed proglacial bedrock indicates continuous Holocene cover, likely by ice. At a nearby smaller glacier, bedrock exposure-burial ages suggest glacier expansion at ~7 thousand years ago, earlier than previously recognized. Moraine exposure ages at these sites and the Sierra Nevada’s largest glacier are distributed across the past several thousand years, suggesting that glaciers were near their preindustrial extent for much of the late Holocene. These findings imply that a glacier-free Sierra Nevada is unprecedented since before the Holocene. Future alpine glacial environments in California are thereby likely a no-analog scenario within the current interglacial.

Keywords

climate change, snowpack, storage, upper watershed management, water supply